The Future of Climate Change
The role of adaptation and mitigation to climate change is described using the concept of planetary boundaries. The future evolution of the main reservoirs of carbon is described. The role of the land and ocean sink, the permafrost feedback and ocean acidification is described. The challenge to keep...
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croxfordunivpr:10.1093/oso/9780198779308.003.0013 2023-05-15T17:50:54+02:00 The Future of Climate Change Adaptation, Mitigation, Geoengineering and Decarbonization Dolman, Han 2019 http://dx.doi.org/10.1093/oso/9780198779308.003.0013 unknown Oxford University Press Biogeochemical Cycles and Climate page 210-226 book-chapter 2019 croxfordunivpr https://doi.org/10.1093/oso/9780198779308.003.0013 2022-08-05T10:30:55Z The role of adaptation and mitigation to climate change is described using the concept of planetary boundaries. The future evolution of the main reservoirs of carbon is described. The role of the land and ocean sink, the permafrost feedback and ocean acidification is described. The challenge to keep Earth’s temperature below 1.5 °C or 2.0 ºC is discussed. As this will involve large amounts of negative emission technologies, such as carbon capture and storage, this may be hard to achieve, as an analysis of their potential and environmental costs shows. Geoengineering has a separate of difficult problems to cope with, which makes the application non-trivial. Decarbonization of societies is discussed and an outline given for a transition path towards a carbon-free society. Book Part Ocean acidification permafrost Oxford University Press (via Crossref) 210 226 |
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Oxford University Press (via Crossref) |
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croxfordunivpr |
language |
unknown |
description |
The role of adaptation and mitigation to climate change is described using the concept of planetary boundaries. The future evolution of the main reservoirs of carbon is described. The role of the land and ocean sink, the permafrost feedback and ocean acidification is described. The challenge to keep Earth’s temperature below 1.5 °C or 2.0 ºC is discussed. As this will involve large amounts of negative emission technologies, such as carbon capture and storage, this may be hard to achieve, as an analysis of their potential and environmental costs shows. Geoengineering has a separate of difficult problems to cope with, which makes the application non-trivial. Decarbonization of societies is discussed and an outline given for a transition path towards a carbon-free society. |
format |
Book Part |
author |
Dolman, Han |
spellingShingle |
Dolman, Han The Future of Climate Change |
author_facet |
Dolman, Han |
author_sort |
Dolman, Han |
title |
The Future of Climate Change |
title_short |
The Future of Climate Change |
title_full |
The Future of Climate Change |
title_fullStr |
The Future of Climate Change |
title_full_unstemmed |
The Future of Climate Change |
title_sort |
future of climate change |
publisher |
Oxford University Press |
publishDate |
2019 |
url |
http://dx.doi.org/10.1093/oso/9780198779308.003.0013 |
genre |
Ocean acidification permafrost |
genre_facet |
Ocean acidification permafrost |
op_source |
Biogeochemical Cycles and Climate page 210-226 |
op_doi |
https://doi.org/10.1093/oso/9780198779308.003.0013 |
container_start_page |
210 |
op_container_end_page |
226 |
_version_ |
1766157827396599808 |